Soil science
Introduction to Soil Science
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Soil is a complex mixture of minerals, organic material, air, and water that supports plant life.
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Soil acts as a medium for plant growth by providing nutrients, anchorage space, and water.
Soil Components
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Minerals form the majority of the soil and come from the breakdown of rocks.
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Organic matter, such as decomposed plant and animal material, is a key source of nutrients for plants.
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Soil water is a primary carrier of nutrients for plant absorption and is essential for biochemical processes.
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Soil air provides the necessary gases for respiration in plants and soil organisms.
Soil Profile and Horizons
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A soil profile refers to the vertical section of soil from the ground surface to the parent rock, divided into layers called horizons.
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The O horizon contains organic matter in various stages of decomposition and is typically dark in colour.
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The A horizon or topsoil is the part of the soil where plants grow most of their roots and is high in organic matter and nutrients.
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The B horizon or subsoil collects minerals leached from the A horizon, is rich in clay, iron, or aluminium compounds.
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The C horizon contains parent material like rocks, and has little organic material or life.
Soil Properties
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Soil texture classifies soil based on the proportion of sand, silt, and clay. Soil texture influences water-holding capacity and nutrient availability.
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Soil structure describes the arrangement of soil particles into aggregates. Good soil structure promotes water movement and root growth.
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Soil colour can indicate its mineral and organic matter content. For instance, dark soil tends to be rich in organic matter.
Soil Water
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The field capacity of soil is the maximum amount of water it can hold after excess water has drained away, crucial for plant growth.
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Wilting point is when the soil has so little water that plants can no longer extract it.
Soil pH and Nutrient Availability
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The pH level of soil affects the solubility of nutrients. Most nutrients are readily available in slightly acidic to neutral soil (pH 6 to 7).
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Soils that are too acidic or alkaline can restrict plant growth due to deficiencies or toxicities of certain nutrients.
Soil Conservation
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Soil erosion is a major environmental concern as it degrades the land’s productivity by removing the nutrient-rich topsoil.
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Practices such as intercropping, mulching, and terracing are effective in preserving soil and preventing erosion.